A 14.7 Ka record of earth surface processes from the arid‐monsoon transitional zone of China

Liu Jianbao; Chen Jianhui; Kandasamy Selvaraj; Chen Shengqian; Xie Chengling; Chen Qiaomei; Lin Baozhi; Yu Kaifeng; Xu Qinghai; Velasco Victor M.; Chen Fahu

摘要

Abstract > The stability of Earth's critical zone is intimately linked with erosion, weathering and vegetation type and density. Therefore, it affects global biogeochemical processes which in turn affect the global climate by absorbing and reflecting solar radiation, and by altering fluxes of heat, water vapour, carbon dioxide and other trace gases through various feedback mechanisms. However, there is a lack of knowledge about how Earth's critical zone processes have changed over time and their link with past monsoon variability, especially in Asia. The study of lake sediments, which contain a suite of inorganic elemental and isotopic proxies, may facilitate the understanding of the Earth's critical zone processes on millennial timescales. Here we reconstruct the history of erosion–weathering–vegetation interactions since ~14.7?ka using geochemical records from a radiocarbon‐dated sediment core from Lake Gonghai in the monsoon‐arid transitional zone of north China. Detrital (Al, Ti, K, Rb) and authigenic (Ca, Sr) elemental records reveal distinct, millennial‐scale, late deglacial‐Holocene erosion and weathering patterns and transitions with the former (latter) elements showing higher (lower) values in warm intervals and <fi>vice versa</fi> . Chemical Index of Alteration (CIA) molar, a humidity proxy, suggests low humidity during the late deglacial ~11.5–14.7?ka, high humidity during the early‐mid Holocene ~11.5–3.2?ka, and intermediate humidity during the late Holocene interval since ~3.2?ka. The results of cross‐spectral analysis and comparison of our records with other climate reconstructions also suggest a pattern of orbitally‐phased humidity changes in north China. Overall, our results provide evidence for the solar‐forcing of Earth's surface processes in mid‐latitude China under natural climatic c </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><abstract xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”xml：lang =“en”> <title type =“main”>抽象</ title> >稳定性地球的关键区与侵蚀，风化和植被类型和密度密切相关。因此，它影响全球生物地球化学过程，这反过来通过吸收和反射太阳辐射来影响全球气候，以及通过各种反馈机制改变热量，水蒸气，二氧化碳和其他痕量气体的助熔剂。然而，缺乏关于地球的关键区域流程如何随时间变化的知识以及与过去的季风变异性，特别是在亚洲的联系。含有一系列无机元素和同位素代理的湖泊沉积物的研究可以促进对千禧一代的临界区流程的理解。在这里，我们重建了自〜14.7的侵蚀 - 风化 - 植被相互作用的历史，从巩膜季风过渡区的拱阳海湖中的无线电铜日沉积物核心中的地球化学记录。贬值（Al，Ti，K，RB）和Authigenic（CA，SR）元素记录揭示了不同的，千年级，晚期的夜间侵蚀和风化图案，与前者（后者）元素的过渡表现出更高（更低）的值温暖的间隔和<fi>反之亦然</ fi>。改变的化学指标（CIA）磨牙，湿度代理，晚期〜11.5-14.7〜11.5-14.7〜11.5-3.2〜11.5-3.2〜11.5-3.2〜11.5-3.2〜11.5-3.2的湿度低湿度〜3.2？ka。与其他气候重建的跨光谱分析和对其记录的比较结果也表明了华北地区的勤勉湿度变化的模式。总体而言，我们的结果为在自然气候C下，在中纬度中国的地球表面流程的太阳能强制迫使地球表面流程提供了证据 </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2018年第3期</span><b style="margin: 0 2px;">|</b><span>共12页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Jianbao&option=202" target="_blank" rel="nofollow">Liu Jianbao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Jianhui&option=202" target="_blank" rel="nofollow">Chen Jianhui;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kandasamy Selvaraj&option=202" target="_blank" rel="nofollow">Kandasamy Selvaraj;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Shengqian&option=202" target="_blank" rel="nofollow">Chen Shengqian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xie Chengling&option=202" target="_blank" rel="nofollow">Xie Chengling;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Qiaomei&option=202" target="_blank" rel="nofollow">Chen Qiaomei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lin Baozhi&option=202" target="_blank" rel="nofollow">Lin Baozhi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yu Kaifeng&option=202" target="_blank" rel="nofollow">Yu Kaifeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Qinghai&option=202" target="_blank" rel="nofollow">Xu Qinghai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Velasco Victor M.&option=202" target="_blank" rel="nofollow">Velasco Victor M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Fahu&option=202" target="_blank" rel="nofollow">Chen Fahu;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Key Laboratory of Western China's Environmental Systems (Ministry of Education)Lanzhou UniversityLanzhou P. R. China;</p> <p>Key Laboratory of Western China's Environmental Systems (Ministry of Education)Lanzhou UniversityLanzhou P. R. China;</p> <p>State Key Laboratory of Marine Environmental Science and Department of Geological OceanographyXiamen UniversityXiamen P. R. China;</p> <p>Key Laboratory of Western China's Environmental Systems (Ministry of Education)Lanzhou UniversityLanzhou P. R. China;</p> <p>Key Laboratory of Western China's Environmental Systems (Ministry of Education)Lanzhou UniversityLanzhou P. R. China;</p> <p>Key Laboratory of Western China's Environmental Systems (Ministry of Education)Lanzhou UniversityLanzhou P. R. China;</p> <p>State Key Laboratory of Marine Environmental Science and Department of Geological OceanographyXiamen UniversityXiamen P. R. China;</p> <p>Department of GeographyRWTH Aachen UniversityAachen Germany;</p> <p>Institute of Nihewan Archaeology Research College of Resources and EnvironmentHebei Normal UniversityShijiazhuang P. R. China;</p> <p>Instituto de Geofísica Universidad Nacional Autónoma de MéxicoCiudad UniversitariaMéxico Mexico;</p> <p>Key Laboratory of Western China's Environmental Systems (Ministry of Education)Lanzhou UniversityLanzhou P. R. China;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Earth's critical zone&option=203" rel="nofollow">Earth's critical zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Earth's surface processes&option=203" rel="nofollow">Earth's surface processes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=arid‐monsoon transitional China&option=203" rel="nofollow">arid‐monsoon transitional China;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Holocene&option=203" rel="nofollow">Holocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=last deglaciation&option=203" rel="nofollow">last deglaciation;</a> </p> <div class="translation"> 机译：地球的关键区;地球的表面流程;干旱季风过渡中国;全新世;最后的解析; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-integrative-plant-biology_thesis/0201255538741.html">沙漠/黄土过渡带13 ka BP以来季风演化的古植被记录</a> <b>[J]</b> . <span> 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W. ,</a> <span>1996</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：1994年1月17日，加利福尼亚州北岭地震期间卡诺加公园，温尼特卡和北岭地区发生共同断层的证据。</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-meteorologica-sinica_thesis/0201254138030.html">中国气候过渡带干旱化发展趋势与东亚夏季风、极涡活动相关研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=廉毅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 廉毅</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=沈柏竹&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,沈柏竹</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=高枞亭&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,高枞亭</a> <span> <a href="/journal-cn-5006/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 气象学报 </a> </span> <span> . 2005</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_quaternary-sciences_thesis/0201253127227.html">岱海沉积记录的季风/干旱过渡区全新世适宜期特征</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙千里&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 孙千里</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=肖举乐&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,肖举乐</a> <span> <a href="/journal-cn-4909/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第四纪研究 </a> </span> <span> . 2006</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_carsologica-sinica_thesis/0201252316544.html">中全新世河南南阳石笋记录的百年季风干旱事件</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=任晓辉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 任晓辉</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=董进国&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,董进国</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈昌海&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,陈昌海</a> <span> <a href="/journal-cn-4822/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国岩溶 </a> </span> <span> . 2006</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_chinese-journal-nature_thesis/020121193841.html">青藏高原北部隆升与东亚季风及亚洲内陆干旱演化——来自气候数值模拟的启示</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘晓东&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘晓东</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=石正国&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,石正国</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郭庆春&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郭庆春</a> <span> <a href="/journal-cn-5253/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 自然杂志 </a> </span> <span> . 2014</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-43375_thesis/020222797120.html">青藏高原东北部新生代地层新进展及其对亚洲干旱-季风系统演化和风化剥蚀记录的控制</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=方小敏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 方小敏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=方亚会&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,方亚会</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨一博&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨一博</a> <span> <a href="/conference-cn-43375/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国矿物岩石地球化学学会第17届学术年会 </a> <span> <span> . 2019</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020311317412.html">石笋记录的中国西南地区97-59ka B.P.期间夏季风的演化</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙喜利&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 孙喜利</a> <span> . 2018</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130458970486.html">Alkaline earth metal salts, transition metal salts and transition metal complexes, coating composition, use of compounds, processes for protecting a metal substrate and for the preparation of metal and product salts</a> <b>[P]</b> . <span> 外国专利：  BR9401407A </span> <span> . 1994-12-13</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：碱土金属盐，过渡金属盐和过渡金属络合物，涂料组合物，化合物的用途，保护金属基材以及制备金属和产品盐的方法 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130433411267.html">It heats processes the rare earth - transition metal type alloy powder, the rare earth - transition metal - nitrogen based alloy powder and</a> <b>[P]</b> . <span> 外国专利：  JP4127128B2 </span> <span> . 2008-07-30</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：加热处理稀土-过渡金属类合金粉末，稀土-过渡金属-氮基合金粉末和 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130470385100.html">METHOD OF ASPHALTOCONCRETE BLANKET AND EARTH DAMS' TRANSITION ZONES CONSTRUCTION FOR WATER CATCHMENT AND EQUIPMENT FOR REALIZATION OF THIS METHOD</a> <b>[P]</b> . <span> 外国专利：  CS253283B1 </span> <span> . 1987-10-15</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：接水用沥青混凝土毛毯和土坝过渡带的施工方法及实现该方法的设备 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023139219','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div 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